|
|
||||||||
ABSTRACT
The effect of drying and rewetting sequences on boron adsorption and desorption by Na- and Ca-montmorillonite suspensions was determined with (i) nondried suspensions, (ii) suspensions dried prior to boron addition, and (iii) suspensions dried once or twice after boron adsorption. Boron adsorption in the nondried suspensions was completely reversible for both the Na- and Ca-systems. There was little effect of exchangeable cation species (Na+ vs. Ca2+) on boron adsorption in the pH values of 7.0 and 7.2. There was a significant exchangeable cation effect, however, at higher pH's, with the Ca-system adsorbing the greatest amount of boron. Boron adsorption on clays dried prior to boron addition was essentially the same for the nondried systems, indicating that the drying and rewetting sequence does not have any effect on the adsorption sites of the clay. The amount of boron adsorbed increased with drying and wetting after boron addition for both the Na- and Ca-systems, with the greatest increase occurring after the first drying-wetting cycle for both systems. Drying and rewetting of the clay suspensions after boron addition not only increased the amount of boron adsorbed, but significantly reduced the reversibility of the adsorption process as well. The relative amount of reversibility of adsorbed boron is a complex function of the drying and rewetting cycles, pH, and type of exchangeable cations.
1 Contribution from the Institute of Soils and Water, Agricultural Research Organization. The Volcani Center, Bet Dagan, Israel. No. 230-E, 1980 series. This research was supported by a grant from the United States-Israel Binational Science Foundation (BSF), Jerusalem, Israel.
2 Soil Scientist, Institute of Soils and Water, ARO, The Volcani Center, Bet Dagan, Israel; and Professor and Head, Department of Agronomy, Univ. of Nebraska, Lincoln, respectively.
Received for publication October 7, 1980. Accepted for publication January 12, 1981.
This article has been cited by other articles:
![]() |
P. J. Vaughan, P. J. Vaughan, and D. L. Suarez Constant Capacitance Model Computation of Boron Speciation for Varying Soil Water Content Vadose Zone J., May 1, 2003; 2(2): 253 - 258. [Abstract] [Full Text] [PDF] |
||||
![]() |
A. Deyhle, A. J. Kopf, and G. Aloisi Boron and boron isotopes as tracers for diagenetic reactions and depth of mobilization, using muds and authigenic carbonates from eastern Mediterranean mud volcanoes Geological Society, London, Special Publications, January 1, 2003; 216(1): 491 - 503. [Abstract] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Vadose Zone Journal | Journal of Plant Registrations | ||||
| Journal of Natural Resources and Life Sciences Education |
Journal of Environmental Quality |
||||